797 resultados para Pittston Strike


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The convergence between the Eurasian and Arabian plates has created a complicated structural setting in the Eastern Turkish high plateau (ETHP), particularly around the Karlıova Triple Junction (KTJ) where the Eurasian, Arabian, and Anatolian plates intersect. This region of interest includes the junction of the North Anatolian Shear Zone (NASZ) and the East Anatolian Shear Zone (EASZ), which forms the northern border of the westwardly extruding Anatolian Scholle and the western boundary of the ETHP, respectively. In this study, we focused on a poorly studied component of the KTJ, the Varto Fault Zone (VFZ), and the adjacent secondary structures, which have complex structural settings. Through integrated analyses of remote sensing and field observations, we identified a widely distributed transpressional zone where the Varto segment of the VFZ forms the most northern boundary. The other segments, namely, the Leylekdağ and Çayçatı segments, are oblique-reverse faults that are significantly defined by uplifted topography along their strikes. The measured 515 and 265 m of cumulative uplifts for Mt. Leylek and Mt. Dodan, respectively, yield a minimum uplift rate of 0.35 mm/a for the last 2.2 Ma. The multi-oriented secondary structures were mostly correlated with “the distributed strike-slip” and “the distributed transpressional” in analogue experiments. The misfits in strike of some of secondary faults between our observations and the experimental results were justified by about 20° to 25° clockwise restoration of all relevant structures that were palaeomagnetically measured to have happened since ~ 2.8 Ma ago. Our detected fault patterns and their true nature are well aligned as being part of a transpressional tectonic setting that supports previously suggested stationary triple junction models.

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The Ivrea–Verbano Zone (IVZ), northern Italy, exposes an attenuated section through the Permian lower crust that records high-temperature metamorphism under lower crustal conditions and a protracted history of extension and exhumation associated partly with the Jurassic opening of the Alpine Tethys ocean. This study presents SHRIMP U–Pb geochronology of rutile from seven granulite facies metapelites from the base of the IVZ, collected from locations spanning ~35 km along the strike of Paleozoic fabrics. Rutile crystallised during Permian high-temperature metamorphism and anatexis, yet all samples give Jurassic rutile U–Pb ages that record cooling through 650–550 °C. Rutile age distributions are dominated by a peak at ~160 Ma, with a subordinate peak at ~175 Ma. Both ~160 and ~175 Ma age populations show excellent agreement between samples, indicating that the two distinctive cooling stages they record were synchronous on a regional scale. The ~175 Ma population is interpreted to record cooling in the footwall of rift-related faults and shear zones, for which widespread activity in the Lower Jurassic has been documented along the western margin of the Adriatic plate. The ~160 Ma age population postdates the activity of all known rift-related structures within the Adriatic margin, but coincides with extensive gabbroic magmatism and exhumation of sub-continental mantle to the floor of the Alpine Tethys, west of the Ivrea Zone. We propose that this ~160 Ma early post-rift age population records regional cooling following episodic heating of the distal Adriatic margin, likely related to extreme lithospheric thinning and associated advection of the asthenosphere to shallow levels. The partial preservation of the ~175 Ma age cluster suggests that the post-rift (~160 Ma) heating pulse was of short duration. The regional consistency of the data presented here, which is in contrast to many other thermochronometers in the IVZ, demonstrates the value of the rutile U–Pb technique for probing the thermal evolution of high-grade metamorphic terrains. In the IVZ, a significant decoupling between Zr-in-rutile temperatures and U–Pb ages of rutile is observed, with the two systems recording events ~120 Ma apart.

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Natural disasters occur in various forms such as hurricanes, tsunamis, earthquakes, outbreaks, etc. The most unsettling aspect of a natural disaster is that it can strike at any moment. Over the past decade, our society has experienced an alarming increase of natural disasters. How to expeditiously respond and recover from natural disasters has become a precedent question for public health officials. To date, the most recent natural disaster was the January 12, 2010 earthquake in Haiti; however the most memorable was that of Hurricane Katrina (“Haiti Earthquake”, 2010). ^ This study provides insight on the need to develop a National Disaster Response and Recovery Program which effectively responds to natural disasters. The specific aims of this paper were to (1) observe the government’s role on federal, state and local levels in assisting Hurricanes Katrina and Rita evacuees, (2) assess the prevalence of needs among Hurricanes Katrina and Rita families participating in the Disaster Housing Assistance Program (DHAP) and (3) describe the level of progress towards “self sufficiency” for the DHAP families receiving case management social services. ^ Secondary data from a cross-sectional “Needs Assessment” questionnaire were analyzed. The questionnaire was administered initially and again six months later (follow-up) by H.A.U.L. case managers. The “Needs Assessment” questionnaire collected data regarding participants’ education, employment, transportation, child care, health resources, income, permanent housing and disability needs. Case managers determined the appropriate level of social services required for each family based on the data collected from the “Needs Assessment” questionnaire. ^ Secondary data provided by the H.A.U.L. were analyzed to determine the prevalence of needs among the DHAP families. In addition, differences measured between the initial and follow-up (at six months) questionnaires were analyzed to determine statistical significance between case management services provided and prevalence of needs among the DHAP families from initial to 6 months later at follow-up. The data analyzed describe the level of progress made by these families to achieve program “self sufficiency” (see Appendix A). Disaster assistance programs which first address basic human needs; then socioeconomic needs may offer an essential tool in aiding disaster affected communities quickly recover from natural disasters. ^

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Detrital modes for 524 deep-marine sand and sandstone samples recovered on circum-Pacific, Caribbean, and Mediterranean legs of the Deep Sea Drilling Project and the Ocean Drilling Program form the basis for an actualistic model for arc-related provenance. This model refines the Dickinson and Suczek (1979) and Dickinson and others (1983) models and can be used to interpret the provenance/tectonic history of ancient arc-related sedimentary sequences. Four provenance groups are defined using QFL, QmKP, LmLvLs, and LvfLvmiLvl ternary plots of site means: (1) intraoceanic arc and remnant arc, (2) continental arc, (3) triple junction, and (4) strike-slip-continental arc. Intraoceanic- and remnant-arc sands are poor in quartz (mean QFL%Q < 5) and rich in lithics (QFL%L > 75); they are predominantly composed of plagioclase feldspar and volcanic lithic fragments. Continental-arc sand can be more quartzofeldspathic than the intraoceanic- and remnant-arc sand (mean QFL%Q values as much as 10, mean QFL%F values as much as 65, and mean QmKP%Qm as much as 20) and has more variable lithic populations, with minor metamorphic and sedimentary components. The triple-junction and strike-slip-continental groups compositionally overlap; both are more quartzofeldspathic than the other groups and show highly variable lithic proportions, but the strike-slip-continental group is more quartzose. Modal compositions of the triple junction group roughly correlate with the QFL transitional-arc field of Dickinson and others (1983), whereas the strike-slip-continental group approximately correlates with their dissected-arc field.

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Structure of assemblages associated with mussel aggregations of Bathymodiolus azoricus was investigated. Mussel beds were found on hydrothermal vent fields on the Mid-Atlantic Ridge (Menez Gwen, Lucky Strike, and Rainbow) at depths 850-2400 m. The community structure of the mussel bed assemblages varied between studied areas. Large number of species was unique to mussel beds of the Menez Gwen field; the most observed taxa were not specialized hydrothermal species. All other nonunique species were found within the Lucky Strike region. The lowest mussel assemblage structure evenness was observed in the shallowest Menez Gwen area (850 m depth). We assume that two types of mussel assemblages (nematode-dominated and copepod-dominated) exist within the Lucky Strike field. The assemblages of B. azoricus differ significantly from assemblages of B. thermophilus inhabiting Pacific hydrothermal vents.

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A morphologically complex igneous basement was penetrated at Leg 125 Site 786 beneath approximately 100 m of Eocene-Pleistocene sediments at 31°52.45 'N, 141°13.59'E in a 3082-m water depth. The site is located on the forearc basement high (FBH) of the Izu-Bonin (Ogasawara) Arc. In the broadest terms, the sequence in Hole 786B consists of a basal sheeted dike complex, heavily mineralized in places, with overlying pillow lavas giving way to a complex and repeated sequence of interlayered volcanic breccias and lava flows with some thin sedimentary intervals. The sequence has been further cut by dikes or sills, particularly of high-Ca and intermediate-Ca boninite, and is locally strongly sheared by faulting. The whole basement has been covered with middle Eocene-early Pleistocene sediments. A monomict breccia forms the shallowest portion of Hole 786B and a polymict breccia having Mn-oxide-rich clast coatings and matrix forms the deepest part of Hole 786A (-100-160 mbsf). The basement is tectonized in some places, and a mineralized stockwork is present in the deepest part of Hole 786B. A wide variety of rock types form this basement, ranging from mafic to silicic in character and including high-, intermediate-, and low-Ca boninites, intermediate- and low-Ca bronzite andesites, andesite, dacite, and rhyolite groups. Intragroup and intergroup relationships are complicated in detail, and several different upper mantle source(s) probably were involved. A significant role for orthopyroxene-clinopyroxene-plagioclase fractionation is indicated in the mafic-intermediate groups, and the most probable complementary cumulates should be noritic gabbros. Many overall similarities but some subtle differences are noted between the igneous basement at Site 786 and the subaerial outcrops of the FBH to the south in the type boninite locality of Chichijima. Both suites were derived by hydrous melting of a relatively shallow, refractory (harzburgitic) upper mantle source. These Bonin forearc basement rocks are similar in many respects to those of Eocene-Oligocene age now forming the forearc of the Marianas at Leg 60 Site 458 and on Guam. In sharp distinction, the geochemistry of the Eocene-Pleistocene ash sequences overlying the Bonin FBH must have been derived from a very different upper mantle source, implying considerable across-strike differences in sub-arc mantle composition.

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Dynamics of the Pacific Plate is recorded in the systematic variation of location and the 40Ar-39Ar age of seamounts in the Western Pacific from 120 to 65 Ma ago. The seamounts are grouped into three linear zones as long as 5000 km. The seamounts become younger in the southeastern direction along the strike of these zones. Correlation between age and location of seamounts allows to divide the history of their formation into three stages. Rate of seamount growth was relatively low (2-4 cm/yr) during the first and the third stages within intervals of 120-90 and 85-65 Ma, whereas during the second stage (90-85 Ma), the seamounts were growing very fast (80-100 cm/yr). In the midst of this stage, at ~87 Ma ago, magmatic activity increased abruptly. Dynamics of seamount building is in good agreement with (1) pulses in development of the Ontong Java, Manihiki, and Caribbean-Colombian oceanic plateaus; (2) age of spreading acceleration in the mid-Cretaceous; and (3) a short period when the Izanagi Plate ceased to exist and the Kula Plate was formed. Variation in seamounts' age and location are in consistence with the hypothesis of diffuse extension of the Pacific Plate in course of its motion with formation of impaired zones of decompression melting. Direction of extension (325°-340° NW) calculated from the strike of seamount zones is consistent with the path of the Pacific Plate (330° NW) in the Late Cretaceous. Immense perioceanic volcanic belts were formed at that time along the margin of the Asian continent. The Okhotsk-Chukchi Peninsula Belt extends at a right angle to the compression vector. Three stages of this belt's evolution are synchronous with the stages of seamount formation in the Pacific Plate. Delay in origination of the East Sikhote-Alin Volcanic Belt and its different orientation were caused by counterclockwise rotation of the vector of convergence of oceanic and continental plates in the mid-Cretaceous. At the same time, i.e. 95-85 Ma ago, volcanic activity embraced the entire continental margin and tin granites were emplaced everywhere in the Eastern Asia. This short episode (90+/-5 Ma) corresponds to the mid-Cretaceous maximum of compression of the continental margin, and its age fits well a culmination in extension of the Pacific Plate.

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El presente trabajo propone explorar el modo cómo la literatura inglesa se apropia de la figura del héroe ático por antonomasia, Teseo, prefiriendo a las historias relacionadas con la aventura aquellas que lo muestran como figura garante del orden y de la sabiduría. Proponemos rastrear el modo cómo el héroe es presentado en el "Cuento del caballero" de los Canterbury Tales, representando no sólo el discurso patriarcal sino y, al mismo tiempo, quien desata las contiendas y quien las re-ordena. En este sentido, la figura del cuento- épico en el sentido bajtiniano del término- testimonia el discurso del orden, donde el varón es el eje vertebrador de la sociedad civil y familiar. Shakespeare, que había tomado contacto con las fuentes clásicas y medievales-tanto italianas como inglesas- incorpora en su Sueño de una noche de verano a un nuevo Teseo, que no sólo discurre acerca de la imaginación sino que también retoma la idea de orden a partir de la proclama de que es necesario someter las trampas de la imaginación a la prueba de la "fría razón". A partir de estos dos ejemplos, trataremos de reflexionar el modo cómo la literatura inglesa se apropió de estos mitos clásicos

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This article aims to analyze the movement of weavers' strike (according to an specific context), its origins, actions and consequences, prompting the internal system of factories (their regulations), the hierarchical relationships of power, and struggles to guarantee the right of association, which resulted in the stoppage of all activities of the textile sector. The attitude to go on a strike, mobilizations and the stroll show that the direction of the movement and the working class were aware of their actions and those likely consequences, what signalize, beforehand, the ideological, classist and political character of women´s actions: radicalized by the practices of confronting the authoritarianism employers and threats (police repression, harassment of the press). They endured through the collective support and a network of solidarity

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En el presente trabajo se estudia el caso de la CGT "disidente" en el período que comprende desde el paro general del 13 de diciembre de 2001 al paro con movilización convocado por dicha organización el 22 de mayo de 2002, el primer intento de paro general y movilización contra el gobierno de Eduardo Duhalde. El objetivo es reconstruir los posicionamientos, prácticas y discursos de la CGT disidente en el proceso socio-histórico señalado, en relación a las medidas político-económicas adoptadas por los gobiernos, frente a las fracciones de empresarios, frente a los proyectos estratégicos en pugna, frente a las otras organizaciones del movimiento obrero organizado y de la clase trabajadora, y con el conjunto del "campo del pueblo". Con ello, se pretende observar la importancia del movimiento obrero organizado, particularmente de la CGT disidente, tanto en la crisis de diciembre de 2001 como en la transición que a partir de allí se abre, durante los primeros meses de la posconvertibilida

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El 2 de mayo de 1928 se inicia una huelga de estibadores portuarios en Rosario después de años de tibia actividad sindical. Días más tarde, varios hechos de sangre provocaron la solidaridad obrera con dos paros generales que conmovieron a la ciudad por su agitación y violencia. Los portuarios villenses también se solidarizaron y, un mes más tarde, encabezaron un violento reclamo laboral. El motivo inicial de las huelgas fue el salarial, pero la cuestión de fondo que hilvana a ambas experiencias es la puja social por el deterioro de las condiciones laborales y las imposiciones empresarias en el control y selección de la fuerza de trabajo.En principio la espontaneidad de la protesta tomó por sorpresa a las organizaciones sindicales de izquierda que durante la década del 20 habían mostraban varias fracturas, no obstante será la oportunidad que explica la reorganización y difusión del movimiento obrero con posterioridad. En otro sentido, los conflictos en Rosario y Villa Constitución reflejan la compleja trama de la política santafesina y su conexión con el ámbito laboral. Asimismo, creemos que los sucesos de 1928 tienen una repercusión mayor que la estrictamente local engarzándose en un ciclo de conflictividad que involucra a buena parte de la economía agroexportadora

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En este artículo, el autor expone las singulares características de la ejecución ilegal de detenidos políticos en una base militar en agosto de 1972, conocida como la «masacre de Trelew¼. También presenta los modos en que esa masacre comenzó a ser recordada en los años siguientes y las lecturas que realizaron de ella las distintas corrientes de izquierda, las cuales no alcanzaron a ver la nueva dimensión del hecho. Finalmente, se pregunta por las relaciones entre este crimen y el terror estatal que sobrevendrá poco tiempo después, como un aporte para reflexionar sobre el concepto de «terrorismo de Estado¼.

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El uruguayo de Copi es un tratado sobre la lengua, una descripción desopilante de un país, un ácido comentario político, una burla impiadosa de los valores culturales, una pesadilla personal, un golpe de teatro donde cualquier versión de la realidad se vuelve precaria y se trastoca al compás de una imaginación afiebrada que no hace más que dar rienda suelta a los materiales del inconsciente. Pero sobre todo, es la visión desnuda de la relación imposible de un escritor con el país que ha dejado atrás. Un tratado sobre el horror de confrontarse con la realidad carcelaria del pasado. Un intento de "calmar" los fantasmas, es decir, de hacerlos hablar y moverse y morir y resucitar en una trama que transita en medio de cadáveres y mares desaparecidos y un territorio que se achica constantemente. Un texto fundamental para indagar cuestiones relacionadas con la "identidad" nacional y con las maneras en que los desplazamientos culturales (con su concomitante tránsito entre lenguas y visiones del mundo), tan comunes en el mundo actual, afectan la escritura.

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El trabajo reflexiona sobre la relación conflictos laborales-huelgas generales en el período 2002-2012 en Argentina a partir del debate Iñigo Carrera-Adrian Piva sobre la huelga general como indicador de los momentos de ascenso y descenso de la lucha de clases, y vinculando dicha relación con algunas discusiones entre las tesis económicas y políticas del conflicto laboral. Incluye una reconstrucción estadística de la conflictividad laboral con datos del Centro de Estudios Nueva Mayoría, Taller de Estudios Laborales y el Ministerio de Trabajo, Empleo y Seguridad Social. Finalmente, reconstruye las huelgas generales a partir de los periódicos Página 12 y La Nación. La relación entre estos tipos de conflicto está históricamente determinada y es por lo tanto, cambiante. En la década se observa desacople mas que coincidencia en ambas protestas, sin embargo, el análisis de las huelgas generales del período cristaliza ciertas transformaciones vividas por el movimiento obrero organizado en nuestro país.

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A mediados de 1919, la ciudad de Buenos Aires se vio conmovida por sucesivas huelgas de los trabajadores y periodistas de los diarios y por un extendido lock-out patronal. Esa crisis desembocó en una situación inédita: durante una quincena, los ciudadanos de Buenos Aires se vieron privados del acceso a los periódicos. El presente trabajo traza el panorama general de la prensa de Buenos Aires en esta coyuntura crítica, y examina los móviles y demandas de los trabajadores, periodistas y empresarios del sector, sus estrategias de acción y las consecuencias del conflicto en el ámbito de la organización sectorial.